Quantifying the high coastal dynamics of tropical mesotidal barrier island-spit systems: case study in Northeast Brazil

  • Filipe Ezequiel da SilvaEmail author
  • Helenice Vital


This study aimed to quantify the morphological variations of the tropical mesotidal barrier-spit systems (MBs) in Northeast Brazil to understand their evolution. Therefore, Landsat 5 TM and Landsat 8 OLI images were used to construct two multitemporal analyses: one in 4-year intervals (low frequency) and another in 1-year intervals (high frequency). The results revealed that the coastal dynamic was so intense that only high-frequency analysis could represent its evolutionary behavior. Low-frequency analysis, on the other hand, could lead to the misinterpretation of the data. Despite the strong coastal dynamic, there was a long-term equilibrium in the areas occupied by the MBs. Furthermore, regarding evolutionary behavior, there were two different types of MBs: migrant and stationary. Migrant MB movement resulted from the joint actions of the meteo-oceanographic forcings that generally push the whole barrier westward, conserving its shape. The migration rate can reach 100 m per year. This process represents the visible and massive movement of sediment along the shore. The changes observed in most MBs, whether migrant or stationary, reflect their ephemeral nature and must serve as a warning for human interventions.


Equatorial coast Coastal erosion Landsat images Multitemporal analysis 



Thanks are due to the GGEMMA group for their survey support, as well as to the PPGG/UFRN for the academic and scientific infrastructure. This is a contribution of INCT AmbTropic – Brazilian National Institute of Science and Technology for Tropical Marine Environments 565054/2010-4, 8936/2011, and 465634/ 2014-1 (CNPq/FAPESB). Finally, we thank the reviewers, whose suggestions significantly improved this paper.

Funding information

Funds for this research were provided by the Higher Education Personnel Improvement Coordination (CAPES) for funding the Master’s scholarship of the first author, the National Council for Scientific and Technological Development (CNPq) for a Research Fellowship (grant PQ 311413/2016–1) to the second author, and the project VALSA (CAPES PVE S).

Supplementary material

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Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  1. 1.Post-Graduate Program in Geodynamics and GeophysicsFederal University of Rio Grande do NorteNatalBrazil
  2. 2.Department of GeologyFederal University of Rio Grande do NorteNatalBrazil

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